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The AAPG/Datapages Combined Publications Database

CSPG Bulletin

Abstract


Bulletin of Canadian Petroleum Geology
Vol. 42 (1994), No. 2. (June), Pages 219-231

A Proposed Global Stratotype for the Second Series of the Ordovician System: Cow Head Peninsula, Western Newfoundland

S. Henry Williams, Felicity H.C. O'Brien, Christopher R. Barnes, W. Douglas Boyce

ABSTRACT

The first occurrence of Tetragraptus approximatus approximatus is now taken to mark the base of the second ("Arenig") series of the Ordovician System. We propose that the Cow Head Peninsula, western Newfoundland, be adopted for Global Stratotype Section and Point (GSSP), with the boundary placed at the base of the T. approximatus Zone, 2.9 m above the base of the Factory Cove Member, Shallow Bay Formation of the Cow Head Group. The well-preserved graptolite fauna occurs in association with abundant conodonts, demonstrating this level to correspond closely with the base of the Prionodus elegans conodont Zone. Immediately underlying strata yield bithecate graptoloid assemblages, generally taken as indicating the latest part of the previous ("Tremadoc") series. Neighbouring sections also yield typically Tremadoc deep-water trilobites from this level, permitting Previous HitcorrelationNext Hit between the three fossil groups. Other fossils, including acritarchs, are also present in the Cow Head Group sections, which are structurally simple, of low thermal maturity (CAI 1.5 or less) and suitable for chemo- and magnetostratigraphic studies.

RESUME

La premiere occurence du Tetragraptus approximatus approximatus sert maintenant a marquer la base de la deuxieme serie ("Arenig") du systeme ordovicien. Nous proposons que la peninsule Cow Head, situee dans la partie ouest de Terre-Neuve, soit adoptee comme coupe et point stratigraphique global (Global Stratotype Section and Point [GSSP]), avec comme limite la base de la zone T. approximatus, 2,9 m au-dessus de la base du membre Factory Cove, de la Formation Shallow Bay du groupe Cow Head. La faune de Graptolites bien conservee de concert avec l'abondance de Conodontes, demontrent que ce niveau correspond de pres avec la base de la Zone de Conodontes Prionodus elegans. La couche directement sous-jacente produit des assemblages de bithecates graptoloides qui indiquent generalement la partie precedente des series anterieures ("Tremadoc"). A ce niveau, les couches avoisinantes produisent typiquement des trilobites en eau profonde Tremadoc permettant ainsi la Previous HitcorrelationTop des trois groupes de fossiles. D'autres fossiles, comme les Acritarches sont egalement presents dans les coupes du groupe Cow Head. Celles-ci sont simples en structure, possedent une maturite thermique basse (CAI 1.5 ou moins) et sont convenables aux etudes chimio- et magnetostratigraphiques.

Traduit par Marie Louise Tomas


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